Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic


Main source = Baratov, R.B., et al. (1976). Subdivisions of stratified and intrusive rocks of Tajikistan. Publishing House "Donish", Dushanbe, 269 pp. plus tables. Provided by Dr. Jovid Aminov, Nazarbayev University, Astana, Kazakhstan Translated to English by the GeoGPT group, Zhejiang Lab, Hangzhou, China--see About

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Kichikhan-Yuly Formation
Click to display on map of the Ancient World at:
Kichikhan-Yuly Fm base reconstruction

Kichikhan-Yuly Fm


Period: 
Jurassic

Age Interval: 
Middle Callovian (J3), Sar2


Province: 
East Tajik (easternmost Pamir)

Type Locality and Naming

Includes in Sarykoln district (Istyk type section (Kokchagin area)

Synonym: Kichikhan-Yuly Suite

Reference section:


Lithology and Thickness

It consists of gray, medium and coarse-bedded nodular clayey limestones. (50 m)


Lithology Pattern: 
Clayey limestone


Relationships and Distribution

Lower contact

Schematic stratigraphic column indicates the lower contact as Kokichegeashui Fm

Upper contact

Schematic stratigraphic column indicates the upper contact as Khan-Yuly Fm

Regional extent

In the Kokchaginsky area, in the basin of the rivers Zhilgakochusu (Kokchagi), Khan-Yuly.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[75.05,37.32],[74.68,37.44],[74.52,37.63],[74.53,37.68],[74.64,37.8],[74.77,37.77],[74.87,37.72],[74.88,37.66],[74.9,37.61],[74.92,37.56],[75,37.5],[75.04,37.51],[75.09,37.44],[75.1,37.41],[75.07,37.38],[75.09,37.33],[75.05,37.32]]]]}}

Fossils

It contains abundant remains of fauna, including the following pteriomorphs: Pinna lanceolata Sow., Plagiostoma streitbergense Orb., P. cf. astartina Thurm., Pseudolimea alternicosta Buv., Lopha eruca Defr., Falcimytilus ex gr. asper Mor. et Lyc.


Age 

Based on the remains of the fauna and its position in the section, the suite is considered Middle Callovian.

Age Span: 

    Beginning stage: 
Callovian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
163.79

    Ending stage: 
Callovian

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
162.66

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Extracted from Baratov, R. B. (1976). Subdivisions of stratified and intrusive rocks of Tajikistan. Donish, Dushanbe, 276.